Km. Lau et al., HYDROLOGIC PROCESSES ASSOCIATED WITH THE FIRST TRANSITION OF THE ASIAN SUMMER MONSOON - A PILOT SATELLITE STUDY, Bulletin of the American Meteorological Society, 79(9), 1998, pp. 1871-1882
Results of a pilot study of the evolution of large-scale hydrologic pr
ocesses associated with the first transition of the Asian summer monso
on in conjunction with the launching of the South China Sea Monsoon Ex
periment (SCSMEX) in May 1998 are presented. SCSMEX is a major interna
tional field experiment to study the water and energy cycles of the As
ian monsoon region, with the aim toward better understanding and impro
ved prediction of the onset, maintenance, and variability of the monso
on of southern China, Southeast Asia, and the western pacific region.
In this paper, the utility of reliable satellite data in revealing cha
racteristics of the South China Sea (SCS) monsoon is emphasized. Using
a combination of satellite-estimated rainfall, moisture, surface wind
, and sea surface temperature, the authors present some interesting an
d hitherto unknown features in large-scale atmospheric and oceanic hyd
rologic processes associated with the fluctuation of the SCS monsoon.
Results show that, climatologically, the SCS monsoon occurs during mid
-May when a major convection zone shifts from the eastern Indian Ocean
-southern Indochina to the SCS. Simultaneous with the SCS monsoon onse
t is the development of a moist tongue and frontal rainband emanating
from the northern SCS, across southern China and the East China Sea to
southern Japan, as well as the enhancement of equatorial convection i
n the western Pacific ITCZ. Analysis of the satellite-derived moisture
and rainfall shows that the onset of the SCS monsoon during 1997 was
preceded by the development of eastward-propagating supercloud cluster
s over the Indian Ocean. The satellite data also reveal a strong onset
vortex over the SCS and large-scale cooling and warming patterns over
the Indian Ocean and western Pacific. These features signal a major s
hift of the large-scale hydrologic cycle in the ocean-atmosphere syste
m, which underpins the SCS monsoon onset. The paper concludes with a b
rief discussion of the observational platform of SCSMEX and a call for
the use of satellite data, field observations, and models for compreh
ensive studies of the Asian monsoon.